使用AE和3D-DIC技术系统检测和评估有缺陷的脆砂岩的裂变行为
PloS one
|September 6, 2024
概括
了解岩石断裂是工程学的关键. 这项研究揭示了岩石破裂期间内部微裂和表面裂如何相互作用,受缺陷方向的影响.
科学领域:
- 地质技术工程 地质技术工程
- 岩石机械学 岩石机械学
- 材料科学 材料科学 材料科学
背景情况:
- 岩石裂变行为对于理解易碎材料中的损伤和断裂过程至关重要.
- 在宏观,微观和表面层面研究裂变,可以全面了解岩石破裂的情况.
研究的目的:
- 在单轴压缩下实验研究有缺陷的砂岩的裂变行为.
- 阐明内部微碎裂和表面裂传播之间的关系.
主要方法:
- 利用声辐射 (AE) 来监测内部微碎裂事件.
- 采用3D数字图像相关性 (3D-DIC) 来追踪表面裂的演变.
- 在单轴压缩下测试了单个预先存在的缺陷的砂岩样本.
主要成果:
- 微裂纹开始并凝聚在一起,在裂纹开始时在表面形成小压力局部化区域 (SLZ).
- 微碎裂合并为宏碎裂,以拉伸或剪切方式传播.
- 缺陷的俯冲角度影响SLZ形成和裂传播方向和模式.
结论:
- 声学和光学数据揭示了缺陷和材料特性如何控制岩石强度和裂机制.
- 这项研究强调了内部微碎裂和岩石质量破裂中的表面裂纹之间的联系.
- 这些发现增强了对脆性岩石裂变过程的理解.
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